Coastal Mo: Difference between revisions

From CSDMS
No edit summary
(Redirected page to Coastal models)
 
(192 intermediate revisions by 5 users not shown)
Line 1: Line 1:
=== Coastal model descriptions===
#redirect [[Coastal_models]]
To submit your model to the list, please complete this questionnaire or email us if you want to update the information about a model that is already listed.
 
{| class="wikitable"
!class="model_topheader_col1"| Model
!class="model_topheader_col2"| Contact Person
!class="model_topheader_col3"| Discussion Page
|}
 
{| class="wikitable collapsible collapsed"
|-
! class="model_header_col1"| sedflux
! class="model_header_col2"| Eric Hutton
! class="model_header_col3"| Not yet
|-
! class="model_section_header" colspan="3" | Contact information
|-
| class="model_col1"| Institute:
| class="model_col2" colspan="2"| University of Colorado
|-
| class="model_col1"| City:
| class="model_col2" colspan="2"| Boulder, CO
|-
| class="model_col1"| Country:
| class="model_col2" colspan="2"| USA
|-
| class="model_col1"| Email:
| class="model_col2" colspan="2"| --
|-
! class="model_section_header" colspan="3" | Model description
|-
| class="model_col1"| Model type:
| class="model_col2" colspan="2"| Modular model
|-
| class="model_col1"| Description:
| class="model_col2" colspan="2"| Sedflux-2.0 is the newest version of the Sedflux basin-filling model. Sedflux-2.0 provides a framework within which individual process-response models of disparate time and space resolutions communicate with one another to deliver multi grain sized sediment load across a continental margin.
|-
! class="model_section_header" colspan="3" | Technical information
|-
| class="model_col1"| Supported platforms:
| class="model_col2" colspan="2"| Unix, Linux, Mac OSX
|-
| class="model_col1"| Programming language:
| class="model_col2" colspan="2"|  C
|-
| class="model_col1"| Model was developed started from:
| class="model_col2" colspan="2"| 1997 and development still takes place
|-
| class="model_col1"| To what degree will the model become available:
| class="model_col2" colspan="2"| As code and as executable
|-
| class="model_col1"| Current license type:
| class="model_col2" colspan="2"| GPL_v2
|-
| class="model_col1"| Memory requirements:
| class="model_col2" colspan="2"| 2GB
|-
| class="model_col1"| Typical run time:
| class="model_col2" colspan="2"| minutes to days
|-
! class="model_section_header" colspan="3" | Input / Output description
|-
| class="model_col1"| Input parameters:
| class="model_col2" colspan="2"| River mouth characteristics (velocity, width, depth, concentration) averaged daily, or longer.
Initial bathymetry.
Input sediment distribution and properties of each grain type.
Optionally, any of: tectonics, sea level, wave climate, and currents
|-
| class="model_col1"| Input format:
| class="model_col2" colspan="2"| ASCII
|-
| class="model_col1"| Output parameters:
| class="model_col2" colspan="2"| Sediment properties that include (but are not limited to) bulk density, grain size, porosity, and permeability.  These are averaged over are user-specified vertical resolution (typically mm to cm).
Sea-floor properties that include slope, water depth, and sand fraction.   
|-
| class="model_col1"| Output format:
| class="model_col2" colspan="2"| Binary
|-
| class="model_col1"| Post-processing software (if needed):
| class="model_col2" colspan="2"| no
|-
| class="model_col1"| Visualization software (if needed):
| class="model_col2" colspan="2"| Yes, Matlab
|-
! class="model_section_header" colspan="3" | Process description
|-
| class="model_col1"| Processes represented by model:
| class="model_col2" colspan="2"| surface plumes, hyperpycnal plumes, sediment slope failure that results in turbidity currents or debris flows, subsidence, compaction, sediment remobilization due to waves and currents, river avulsion
|-
| class="model_col1"| Key physical parameters & equations:
| class="model_col2" colspan="2"| Too numerous to list.
|-
| class="model_col1"| Length scale & resolution constraints:
| class="model_col2" colspan="2"| Vertically: mm to cm; Horizontally: 10s of m to 1000 of m
|-
| class="model_col1"| Time scale & resolution constraints:
| class="model_col2" colspan="2"| Days or greater. Component processes can have much higher resolutions for numerical stability.
|-
| class="model_col1"| Numerical limitations and issues :
| class="model_col2" colspan="2"| --
|-
! class="model_section_header" colspan="3" | Testing
|-
| class="model_col1"| Available calibration data sets:
| class="model_col2" colspan="2"| --
|-
| class="model_col1"| Available test data sets:
| class="model_col2" colspan="2"| --
|-
| class="model_col1"| Ideal data for testing:
| class="model_col2" colspan="2"| --
|-
| class="model_section_header" colspan="3" | User groups
|-
| class="model_col1"| Currently or plans for collaborating with:
| class="model_col2" colspan="2"| None
|-
! class="model_section_header" colspan="3" | Documentation
|-
| class="model_col1"| Key papers of the model:
| class="model_col2" colspan="2"|  Sedflux-2.0: An advanced process-response model that generates three-dimensional stratigraphy.
|-
| class="model_col1"| Is there a manual available:
| class="model_col2" colspan="2"|  Yes
|-
| class="model_col1"| Model website if any:
| class="model_col2" colspan="2"| [[http://sedflux.googlecode.com|http://sedflux.googlecode.com]]
|-
! class="model_section_header" colspan="3" | Additional comments
|-
| class="model_col1"| Comments:
| class="model_col2" colspan="2"|  No
|}

Latest revision as of 11:16, 30 August 2012

Redirect to: